Download clay - College of Charleston

Let’s Play with Clay in the Piedmont
(First Draft)
Focus Questions
Why do you find such big rivers in the Piedmont region of South Carolina? Why is the
water in these rivers often reddish-colored?
Activity Synopsis
During this activity, students will conduct an experiment using clay and sand to
understand why there are so many big rivers in the Piedmont region of South Carolina.
Students will also learn why Piedmont rivers are often reddish-colored.
Time Frame
One hour
Student Key Terms
 clay
 piedmont
 run off
 sand
 impermeable
 permeable
Objectives
The learner will be able to:
 Conduct an experiment in which he/she observes how water travels through
clay and through sand.
 Explain that run off from the clay soils of the Piedmont region creates large
rivers in that region.
Third Grade Standards Addressed
Science Standards
IIC2a; IIIA1b,c,d
Background
Key Points
Key Points will give you the main information you should know to teach the activity.
 The Piedmont region of South Carolina is a region of rolling hills and red
rivers that make up about one-third of our state and extends from the Sandhills
From COASTeam Aquatic Workshops: the Piedmont (Grade 3); a joint effort between the COASTeam
Program at the College of Charleston and the South Carolina Aquarium – funded by the SC Sea Grant
Consortium.
1
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in Columbia to the Mountains (the term “piedmont” actually means the “foot
of the mountains” in French).
The rivers of the Piedmont are red, because the soil of the Piedmont is red.
The soil of the Piedmont consists primarily of clay with high iron content.
When iron comes in contact with oxygen it turns red (this is what happens
when cars up north rust), so the soils of the Piedmont are reddish-orange in
color.
Porosity is the amount of water a substance can hold or, in other words, the
amount of space available in the substance that can hold water. It is expressed
as a percentage.
Permeability refers to the ease at which water passes through a substance.
In soils, large sediment sizes tend to have more spaces between them and so
have a higher porosity and permeability.
Sand has much larger particle sizes than clay.
On soils with large sediment sizes the water in rain is more likely to become
groundwater. On soils with small sediment sizes, the water is more likely to
become surface runoff.
Because the Sandhill soils are made primarily of sand and have high porosity
and permeability, the rain that falls on them is most likely to soak into the
ground and become groundwater.
Because the Piedmont soils are made primarily of clay and have low porosity
and permeability, almost all rain that falls in the Piedmont region runs off.
This, combined with the large amounts of water flowing in from the Mountain
regions of both South and North Carolina, creates the large rivers that
characterize this region. These rivers include the Savannah, Broad, Saluda and
Catawba rivers. Each of these rivers flows eastward towards the Atlantic
Ocean.
Detailed Information
Detailed Information gives more in-depth background to increase your own knowledge,
in case you want to expand upon the activity or you are asked detailed questions by
students.
The Piedmont region of South Carolina is a region of rolling hills and red rivers
that make up about one-third of our state and extends from the Sandhills in Columbia to
the Mountains (the term “piedmont” actually means the “foot of the mountains” in
French). Elevation drops across the Piedmont from the base of the Mountains (about
1200 feet in elevation) to the Sandhills (about 300 feet in elevation). The area where the
underlying rock of the Piedmont meets the underlying rock of the Coastal Plain in the
Sandhills is called the “fall line”. Because the rock of the Piedmont is higher and more
resistant to erosion than the rock of the Coastal Plain, the water literally “falls” here and
“fall line” is an area of rocky, rapid-moving water.
The rivers of the Piedmont are red, because the soil of the Piedmont is red. The
soil of the Piedmont consists primarily of clay with high iron content. When iron comes
in contact with oxygen it turns red (this is what happens when cars up north rust), so the
From COASTeam Aquatic Workshops: the Piedmont (Grade 3); a joint effort between the COASTeam
Program at the College of Charleston and the South Carolina Aquarium – funded by the SC Sea Grant
Consortium.
2
soils of the Piedmont are reddish-orange in color. Sandhills soils, on the other hand, are
made up of sand. The clay-rich soils of the Piedmont are not very porous or permeable,
while Sandhill soils are very porous and permeable.
Porosity is the amount of water a substance can hold or, in other words, the
amount of space available in the substance that can hold water. It is expressed as a
percentage. Permeability refers to the ease at which water passes through a substance.
In soils, large sediment sizes tend to have more spaces between them and so have a
higher porosity and permeability. Sand has much larger particle sizes than clay.
Because the Sandhill soils are made primarily of sand and have high porosity and
permeability, the rain that falls on them is most likely to soak into the ground and become
groundwater. Because the Piedmont soils are made primarily of clay and have low
porosity and permeability, the rain that falls on them is most likely to become surface
runoff. On soils with large sediment sizes the water in rain is more likely to become
groundwater. On soils with small sediment sizes, the water is more likely to become
surface runoff.
When it rains, the water dissipates in various ways. Some of the water seeps into
the ground while some of it runs off to nearby rivers and streams, some of the water is
absorbed by plants and some of it evaporates back into the atmosphere. Depending on
where you are, the visible results of this will vary. In some areas of South Carolina, such
as the Sandhills, it can rain all day and when it stops there are very few signs of the recent
deluge of water. In other areas, such as downtown Charleston, it rains just a little and cars
have to plow through three feet of water. What is the difference? Though there are many
factors involved, one of the main things that affects the ratio between water saturation
and water runoff is the porosity and permeability of the soil.
When it rains, the water is pulled down by gravity through the spaces between the
soil particles and the cracks and fissures in the rocks. This water is known as
groundwater. It is estimated that 95% of all freshwater available and approximately 50%
of the water Americans drink is found in groundwater. Generally, groundwater is found
within 100 meters of the surface.
The amount of water that can be held by the soil is known as its porosity. Porosity
is the ratio between empty spaces in the soil and the soil itself. It is expressed as a
percentage. For example, if 30% of a volume of soil is open space then 30% of it can
contain water and thus it has a porosity of 30%. A liter (1000ml) of soil with a porosity of
30% can contain approximately 300ml (30% of a liter) of water.
Permeability is the rate at which water will flow through the soil to become part
of the zone of saturation. Soils with high permeability allow water to flow through them
very quickly. Soils and surfaces with low permeability do not allow water to flow
through them very well, and have higher amounts of surface runoff.
Both porosity and permeability are affected by the particle size of the soil.
Though all soil particles are small, there are microscopic differences in size. Very coarse
grained- particles, 60 mm in diameter or larger, are characterized as cobbles and
boulders. Coarse-grained particles, 2 to 60 mm, are classified as gravel. Medium-grained
particles, 0.06 to 2 mm, are classified as sand. Fine-grained particles, 0.002 to 0.06 mm,
are classified as silt. Very fine-grained particles, less than 0.002 mm, are classified as
clay. Soils with relatively large particle sizes, such as sand and gravel, have larger gaps
From COASTeam Aquatic Workshops: the Piedmont (Grade 3); a joint effort between the COASTeam
Program at the College of Charleston and the South Carolina Aquarium – funded by the SC Sea Grant
Consortium.
3
between their particles and thus have a higher porosity. These
gaps also allow a quicker transfer of water leading to a higher
permeability. Soils with small particle sizes, such as clay, have
very tiny open spaces and thus have low porosity and
permeability. Because soil is often a mixture of different
sediment sizes, this can affect the porosity of the soil. Small
particle size sediment can sometimes fill the gaps between
large particle size sediment, thus lowering porosity.
Soils are mixtures of gravel, sand, silt, clay and organic material. The texture of
soils is characterized by the percentages of sediment particle sizes in its make-up. It can
be predominately sand, predominately clay, fairly even mixtures of both or various other
combinations. Soils in South Carolina are composed primarily of sand or clay, and so are
sandy or clay soils.
Sandy and clay soils have very different properties. Because of their larger
particle size, sandy soils have a higher porosity and permeability. Water drains through
them quickly, and they have more capacity to contain water. Because of the relatively
large gaps between their grains, though, water loses its cohesive property and sand cannot
hold water in its zone of aeration. For this reason, the topsoil of sandy soils tends to be
well aerated, but very dry.
Clay soils have a smaller particle size, and thus have a lower porosity and
permeability. Water drains very slowly, most of it running off before it can seep through.
Because of the tiny gaps between the small clay particles, water that does seep through is
held in the clay by cohesion. This is what gives clay its slimy, sticky feel. Because clay
soils hold water so well, they become almost completely saturated with water and there is
little space for air to infiltrate the clay. For this reason, clay soils are very moist soils, but
not well aerated.
In South Carolina, the sediment types found in major regions affect saturation to
runoff ratios. Each of these regions can be encountered in the Santee River watershed. In
the Blue Ridge Mountain region of the state, the soil layer is very thin, with impermeable
rock close to the surface. The Mountain region has the highest rainfall rate in the state,
averaging over 60 inches a year. Because of the high amount of rainfall and the small
amount of soil that can be saturated, most of the rain that hits the mountains becomes run
off. This run off manifests itself in the streams and waterfalls found throughout the
mountain region.
The streams of the Mountain region flow into the rivers of the Piedmont region.
The soil layer in the Piedmont region is much thicker than that of the Mountain region. It
is soil made up of sediment eroded from the mountains and is composed primarily of
clays. Clays have the smallest particle size, and for this reason are virtually impermeable
to water. Because of the impermeability of the soil, almost all rain that falls in the
Piedmont region runs off. This, combined with the large amounts of water flowing in
from the Mountain regions of both South and North Carolina, creates the large rivers that
characterize this region. These rivers include the Savannah, Broad, Saluda and Catawba
rivers. Each of these rivers flows eastward towards the Atlantic Ocean.
Midway through the state, these rivers cross the Sandhills, the boundary between
the Piedmont and the Coastal Plain. The Sandhills are the remnants of ancient sand
From COASTeam Aquatic Workshops: the Piedmont (Grade 3); a joint effort between the COASTeam
Program at the College of Charleston and the South Carolina Aquarium – funded by the SC Sea Grant
Consortium.
4
dunes, formed when the ocean reached this part of the state about 9 to 12 million years
ago during the Miocene Epoch. As can be gathered from the name, Sandhill soils are
composed primarily of sand. Sand has a much larger particle size than clay,
approximately the same size difference as a basketball has to a golf ball. Because of the
large size of its particles, the soil is looser and has more open space for water transport
and so has a very high permeability. When it rains in the Sandhills, almost all of the
water quickly soaks into the ground. Because the soil cannot hold water for very long, it
resembles a desert because the topsoil is so dry. Only vegetation adapted to this type of
habitat, such as cacti and briars, grows there.
Past the Sandhills, the rivers enter the Coastal Plain. The Coastal Plain is a region
of sand, clay and limestone characterized by large winding rivers and large areas of
wetlands. The soil is the result both of the sediment brought in by the ancient oceans, and
the sediment brought in and deposited by the rivers from the Mountain and Piedmont
region that is still occurring today. The sand and limestone both have a high porosity, and
with the impermeable clays around them keeping the water in place, they act as aquifers,
porous bodies of rock that allow water to pass through easily, for the majority of South
Carolina’s groundwater.
The Coastal Plain is also characterized by many wetlands. Wetlands and
groundwater have an important relationship. Wetlands collect and hold water that
recharges the groundwater. They also return the favor by being receptors for large
amounts of water discharged from the groundwater.
With the spread of human populations, and the increase in construction of
buildings, roads and parking lots, humans have thrown a wrench into the
groundwater/runoff works. Almost any human construction creates an impermeable
surface, a surface that water cannot run through, decreasing the amount of surface area
that water can infiltrate, and causing rainwater to run off. As pavement is often covered
with contaminants such as garbage and oil spilled by cars, these contaminants are picked
up by the runoff water and carried to streams and other bodies of water, and are a major
source of non-point pollution.
Runoff of impermeable surfaces is a particular problem in urban areas. The
concentration of development not only increases the problems of water contamination,
but also creates problems with flooding. Having no permeable surfaces causes the
rainwater to run in the streets. To prevent flooding in the streets, cities construct storm
sewers that drain the streets and discharge the water into nearby streams. This sudden
expulsion of urban water in the streams often leads to flooding, contamination by
pollutants and rapid temperature increases from water off of sun-heated roads. In
Charleston, SC, the high water table, brought on by the close proximity of the city to the
ocean and to two major rivers (the Ashley and the Cooper) and the fact that most of the
city was built on wetland areas, causes the storm sewers to be ineffectual, as they are
already filled with water. When it rains, many streets fill up with one, two and even three
feet of water and suddenly amphibious cars do not seem like such a bad idea.
From COASTeam Aquatic Workshops: the Piedmont (Grade 3); a joint effort between the COASTeam
Program at the College of Charleston and the South Carolina Aquarium – funded by the SC Sea Grant
Consortium.
5
Procedures
Materials
Per group of four students:
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Clay (clay that is not water-based)
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Container for water
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Water
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Cylindrical funnel
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Nylon netting or pantyhose
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Rubberband
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Container to catch water flowing through funnel
Procedure
1. Introduce this activity by having the students observe what happens to the
water that is poured onto the soil of a potted plant. Does it all seep into the soil
at once? Does some of it sit on top? What would happen to the water that sits
on top if you tilted the plant at an angle? Does it run off? What happens to
rain that falls on the ground? What happens to rain that falls on grassy areas?
What happens to rain that falls on a slide? Does it soak into the slide? Where
does it go? Discuss the questions and observations with the students and write
their thoughts and ideas on the board.
2. Introduce the concept of runoff to the students. Explain that water soaks into
some materials but not into others. For example, water will soak into a grassy
area until the soil below the grass is completely soaked with water. Water that
falls onto the glass window of a car, however, rolls down off of the window.
The water that lands on the car window does not soak into the window.
3. Tell students that they are about to conduct an experiment in which they
observe how water travels through sand and through clay.
4. Ask students to stretch nylon netting along the bottom of their funnel and to
wrap it around with a rubber band.
5. Once the netting is in place, have students place their funnels over a container
and fill their funnels with approximately 100mls of sand.
6. Have students measure 200 ml of water and pour the water into the funnel.
From COASTeam Aquatic Workshops: the Piedmont (Grade 3); a joint effort between the COASTeam
Program at the College of Charleston and the South Carolina Aquarium – funded by the SC Sea Grant
Consortium.
6
7. Ask students what they observed. Did the water travel through quickly or
slowly?
8. Ask students to remove the sand from their funnel, to rinse the funnel and to
dry the funnel completely.
9. Have students fill the funnel with 100 ml of clay and repeat the procedure
used with the sand. Make sure students knead the clay into the funnel so no
large spaces exist along the edges. Demonstrate this step, if needed.
10. After students to pour 200 milliliters of water on the clay, ask them what they
observed. Did the water travel through the clay quickly, slowly or not at all?
11. Explain that clay particles are much tinier than sand particles and that because
clay particles are so small, they sit tightly together and do not allow much
water to soak into them or to travel through them.
12. Ask students what they think would happen to rain that falls onto a sandy
area. Ask students what they think would happen to rain that falls onto an area
made of clay.
13. Ask students to recall what they learned about the Piedmont region from their
Sculpting South Carolina activity.
14. Remind students of the following, if needed: , the Piedmont topography is
characterized by rolling hills and valleys with moderate slopes. Elevation
ranges from 300 feet to 1400 feet and descends closer to the coast. Soils
consist primarily of red and yellow clays. The streams of the Mountains, as
well as rainwater runoff on the impermeable clay of the Piedmont, join
together to form large rivers in the Piedmont. Average annual rainfall ranges
between 46 and 54 inches.
15. Using probing questions, lead students to the following conclusion: since the
Piedmont region is made up of clay and water does not soak into clay or travel
very well through clay, when it rains in the Piedmont, water just runs off of
the clay and down hills to valleys where large rivers are formed.
Assessment
Tell students they have to buy a home. Ask students to circle the home they would prefer
to buy using the drawing provided below and to explain their choice. Let students know
that they are purchasing the home during a season with very, very heavy rain fall and that
flooding, in some areas along the river, has occurred in past years. Both homes are
located right on the banks of the Giant river. Home A is built on clay soil while home B
is built on sandy soil.
From COASTeam Aquatic Workshops: the Piedmont (Grade 3); a joint effort between the COASTeam
Program at the College of Charleston and the South Carolina Aquarium – funded by the SC Sea Grant
Consortium.
7
Members of the COASTeam Aquatic Workshops development team include: Katrina Bryan,
Jennifer Jolly Clair, Stacia Fletcher, Kevin Kurtz, Carmelina Livingston, and Stephen Schabel.
From COASTeam Aquatic Workshops: the Piedmont (Grade 3); a joint effort between the COASTeam
Program at the College of Charleston and the South Carolina Aquarium – funded by the SC Sea Grant
Consortium.
8
A
B
From COASTeam Aquatic Workshops: the Piedmont (Grade 3); a joint effort between the COASTeam
Program at the College of Charleston and the South Carolina Aquarium – funded by the SC Sea Grant
Consortium.
9